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Figure 7: Observed chemical reactivity at Montmiral: large secondary pore in corroded Kfeldspar<br />
that is part of a coarse lithic grain, which is infilled by fine grained moderately<br />
developed kaolinite books (Q = quartz, F = feldspar, D = dolomite, k = kaolinite, Fe = Fe<br />
oxyhydroxides, S = siderite, M = mica) (Riding and Rochelle, 2005).
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